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Anomalies observed in VLF and LF radio signals on the occasion of the western Turkey earthquake (Mw = 5.7) on May 19, 2011

机译:2011年5月19日土耳其西部地震(Mw = 5.7)时在VLF和LF无线电信号中观察到异常

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摘要

Since 2009 a network of VLF (20 - 60 kHz) and LF (150 - 300 kHz) radio receivers is operating in Europe in order to study the disturbances produced by the earthquakes on the propagation of these signals. In 2011 the network was formed by nine receivers, of which three are located in Italy and one is in Austria, Greece, Portugal, Romania, Russia and Turkey. On May 19, 2001 an earthquake (Mw = 5.7) occurred in western Turkey, that is inside the “sensitive” area of the network. The radio data collected during April-May 2011 were studied using the Wavelet spectra, the Principal Component Analysis and the Standard Deviation trends as different methods of analysis. Evident anomalies were revealed both in the signals broadcasted by the TRT transmitter (180 kHz) located near Ankara and in a VLF signal coming from a transmitter located in Western Europe and collected by the receiver TUR of the network located in eastern Turkey. Evident precursor phases were pointed out. Some differences in the efficiency of the three analysis methods were revealed.
机译:自2009年以来,VLF(20-60 kHz)和LF(150-300 kHz)无线电接收器网络已在欧洲运行,以研究地震对这些信号的传播产生的干扰。 2011年,该网络由九个接收方组成,其中三个位于意大利,一个位于奥地利,希腊,葡萄牙,罗马尼亚,俄罗斯和土耳其。 2001年5月19日,土耳其西部发生地震(Mw = 5.7),该地震发生在该网络的“敏感”区域内。使用小波频谱,主成分分析和标准偏差趋势作为不同的分析方法,研究了2011年4月至5月收集的无线电数据。在安卡拉附近的TRT发射机(180 kHz)广播的信号以及在西欧的发射机发出的VLF信号中均发现了明显的异常,该信号由位于土耳其东部的网络的接收机TUR收集。指出了明显的前体相。揭示了三种分析方法在效率上的一些差异。

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